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Pikes Peak granite is a 1.08 billion year old Late-Precambrian geologic formation found in the central part of the Front Range of Colorado. It is a coarse-grained pink to light red syenogranite with minor gray monzogranite , and it has a distinctive brick-red appearance where it outcrops.
Pikes Peak seen from the Garden of the Gods. The Pikes Peak region is renowned for its rare mineral specimens. It is a favorite collecting area for amateur and serious rock hounds. Scientists from around the world come to Colorado to study the minerals of this region.
Pikes Peak is the highest summit of the southern Front Range of the Rocky Mountains in North America.The ultra-prominent 14,107-foot (4,299.83 m) fourteener is located in Pike National Forest, 12 miles (19 km) west of downtown Colorado Springs, Colorado.
The outstanding geologic features of the park, including Steamboat Rock, the Three Graces, and Balanced Rock, are the ancient sedimentary beds of deep-red, pink and white sandstones, conglomerates and limestone that were deposited horizontally, but have now been tilted vertically and faulted into "fins" by the immense mountain building forces caused by the uplift of the Rocky Mountains and the ...
The Paleozoic era and during the Precambrian eon, about 300 million to one billion years ago, Pikes Peak Granite was formed from mass amounts of molten rock that would amalgamate, flow and combine, to form the continents. In Colorado it is known as the Precambrian Pikes Peak Granite.
The Pike National Forest is located in the Front Range of Colorado, United States, west of Colorado Springs including Pikes Peak. The forest encompasses 1,106,604 acres (4,478 km 2) within Clear Creek, Teller, Park, Jefferson, Douglas and El Paso counties. The major rivers draining the forest are the South Platte and Fountain Creek.
Devil's Head Lookout is a U.S. Forest Service fire lookout tower at the summit of Devils Head in Douglas County, Colorado.Located on a large pinnacle of Pikes Peak granite, the fire lookout point lies within the Pike National Forest and is accessed by hiking the Devils Head National Recreation Trail.
About 500 million years ago during the Ordovician period warm shallow seas covered the Pikes Peak region of Colorado. The seas were home to abundant shell creatures that accumulated on the sea floor when they died. The layers built up for millions of years and were eventually compacted and hardened into the rock known as limestone.